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Local Earthquake Magnitude Scale and B‐Value for the Danakil Region of Northern Afar

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Local Earthquake Magnitude Scale and B‐Value for the Danakil Region of Northern Afar Illsley-Kemp, F., Keir, D., Bull, J. M., Ayele, A., Hammond, J., Kendall, J. M., Gallacher, R. J., Gernon, T., & Goitom, B. (2017). Local Earthquake Magnitude Scale and b‐Value for the Danakil Region of Northern Afar. Bulletin of the Seismological Society of America, 107(2), 521-531. https://doi.org/10.1785/0120150253 Publisher's PDF, also known as Version of record Link to published version (if available): 10.1785/0120150253 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Seismological Society of America at DOI: 10.1785/0120150253. Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Bulletin of the Seismological Society of America, Vol. 107, No. 2, pp. 521–531, April 2017, doi: 10.1785/0120150253 Ⓔ Local Earthquake Magnitude Scale and b-Value for the Danakil Region of Northern Afar by Finnigan Illsley-Kemp, Derek Keir,* Jonathan M. Bull, Atalay Ayele, James O. S. Hammond, J.-Michael Kendall, Ryan J. Gallacher, Thomas Gernon, and Berhe Goitom Abstract The Danakil region of northern Afar is an area of ongoing seismic and volcanic activity caused by the final stages of continental breakup. To improve the quantification of seismicity, we developed a calibrated local earthquake magnitude scale. The accurate calculation of earthquake magnitudes allows the estimation of b-values and maximum magnitudes, both of which are essential for seismic-hazard analysis. Earthquake data collected between February 2011 and February 2013 on 11 three-component broadband seismometers were analyzed. A total of 4275 earthquakes were recorded over hypocentral distances ranging from 0 to 400 km. A total of 32,904 zero-to-peak amplitude measurements (A) were measured on the seismometer’s horizontal components and were incorporated into a direct linear inversion that M solved for all individual local earthquake magnitudes ( L), 22 station correction fac- C n K M A− tors ( ), and 2 distance-dependent factors ( , ) in the equation L log log A0C. The resultant distance correction term is given by − log A0 1:274336 log r=17 − 0:000273 r − 172. This distance correction term suggests that attenuation in the upper and mid-crust of northern Afar is relatively high, con- sistent with the presence of magmatic intrusions and partial melt. In contrast, attenu- ation in the lower crust and uppermost mantle is anomalously low, interpreted to be caused by a high melt fraction causing attenuation to occur outside the seismic fre- M quency band. The calculated station corrections serve to reduce the L residuals sig- nificantly but do not show a correlation with regional geology. The cumulative seismicity rate produces a b-value of 0:9 0:06, which is higher than most regions of continental rifting yet lower than values recorded at midocean ridges, further sup- porting the hypothesis that northern Afar is transitioning to seafloor spreading. Electronic Supplement: List of all local earthquakes used in the study with calculated local magnitudes and associated magnitude error. Introduction The Danakil region, in northern Afar, is one of the few analysis, in particular when estimating b-values and maximum areas in the world where the transition from continental rifting magnitudes. Accurate local magnitudes are also essential for to seafloor spreading is exposed subaerially. The region is seis- studies that attempt to understand the geological processes oc- mically active and encompasses at least 24 active volcanic curring in locations such as northern Afar, for example, stress centers. The Ethiopian plateau, to the west of the Danakil de- accumulation and amount of strain by faulting. pression, supports a significant population. Given its proximity Seismic energy will attenuate at varying rates depending to the western border fault of Afar, the town of Mekele faces a on factors such as temperature, composition, and fluid high level of seismic risk and experienced a swarm of earth- content of the crust as well as partial melt and magmatic in- quakes in 2002 (Ayele et al.,2007). The accurate calculation trusions (Schlotterbeck and Abers, 2001; Carletti and Gas- of local magnitudes is a key component of seismic-hazard perini, 2003; Keir et al., 2006; Wang et al., 2009). This rate of attenuation is characterized by an attenuation curve. *Also at the Dipartimento di Scienze della Terra, Università degli Studi di The use of an inappropriate attenuation curve will result in Firenze, Florence, Italy. errors when assigning local magnitude values to earthquakes. 521 522 F. Illsley-Kemp, D. Keir, J. M. Bull, A. Ayele, J. O. S. Hammond, J.-M. Kendall, R. J. Gallacher, T. Gernon, and B. Goitom Figure 1. The seismic network deployed for this study. The network was in place between February 2011 and February 2013. Stations marked with asterisks had one or more faulty horizontal components and so were not used for calculating magnitudes. The region contains the Erta-Ale volcanic segment (EAVS), the Dabbahu volcanic segment (DVS), Nabro volcano (NVS), the Amarta-Barawli volcanic complex (ABVS), Afdera volcano (AV), and Alayta volcano Figure 2. Locations and respective magnitudes of the 4275 (ALV). Topography data were taken from National Aeronautics and earthquakes recorded in the two years between February 2011 Space Administration (NASA)’s Shuttle Radar Topography Mission. and February 2013. All earthquakes have a minimum of four phases recorded on a minimum of three stations. The black box outlines For two years, from 2011 to 2013, a seismic network was those earthquakes associated with the eruption of Nabro volcano. 260 150 deployed over an area covering × km (Figs. 1 ∼20 = and 2). The goal of this study is to use the seismic data re- mm yr in the south (13° N), with the extension – corded by 11 broadband seismometers to quantify seismic directed east-northeast west-southwest (McClusky et al., activity including improved estimation of local magnitudes 2010). The crust thins dramatically in the Danakil depres- ∼27 (M ). To do this, we invert maximum body-wave amplitude sion from km thickness in the rift to the south of the L <15 and hypocentral distance information to derive a region- depression to km beneath the depression (Makris and specific magnitude scale based on the definitions of Richter Ginzburg, 1987; Hammond et al.,2011). The crust is >40 (1935, 1958). km thick beneath the Ethiopian plateau (Hammond et al., 2011; Corti et al., 2015). The Danakil depression is an ∼200-km long 50–150-km Geological Setting wide basin that is mostly below sea level but currently sub- The Afar depression is a region that is in the late stages aerial (Fig. 1). Because of the low elevation, the surface sedi- of continental breakup and lies at the triple junction be- ments in the area largely consist of thick layers of evaporites tween the Gulf of Aden, the southern Red Sea, and the formed from repeated marine incursions (Barberi and Varet, Main Ethiopian rift (McKenzie and Davies, 1970; Mohr, 1970; Keir et al., 2013), most recently 32,000 years ago 1970). The initiation of rifting in Afar occurred between (Bonatti et al., 1971). The depression also contains the 31 and 29 Ma (Hofmann et al., 1997; Ukstins et al., NNW–SSE-trending Erta-Ale volcanic segment (EAVS) and 2002), with initial extension thought to be accommodated seven active volcanoes (Barberi and Varet, 1970; Nobile by large-scale border faults (Wolfenden et al., 2005). In et al., 2012; Fig. 1). The volcanic range is the focus for most northern Afar, strain localized to north-northwest–south- of the magmatic activity in the region and is responsible for southeast (NNW–SSE)-trending 10–30-km-wide 60–100- the majority of Quaternary to recent basalts in Afar (Bastow km-long axial volcanic segments between 25 and 20 Ma and Keir, 2011). It is also thought to mark the boundary of (Hayward and Ebinger, 1996; Wolfenden et al., 2005). the Danakil microplate to the east (Eagles et al., 2002). Geo- Extension rates vary across the Danakil region, with exten- detic observations of Gada-Ale, Dallol, and Alu-Dalafilla sion of ∼7 mm=yr in the northernmost area (15° N) and volcanoes in the Erta-Ale range have been successfully mod- Local Earthquake Magnitude Scale and b-Value for the Danakil Region of Northern Afar 523 0 100 200 300 400 500 eled as fluxes of magma in upper-crustal reservoirs and in- 4000 trusions (Amelung et al., 2000; Field et al., 2012; Nobile Frequency et al., 2012; Pagli et al., 2012). Density 2000 In addition to the Erta-Ale volcanic range, there are a suite of other active volcanoes in the region (Fig. 1). At the southern 4000 2000 edge of the Danakil depression, there are the Amarta-Barawli 6 6 volcanic complex (ABVS), Afdera volcano (AV), and Alayta volcano (ALV) (Barberi and Varet, 1970). To the south of the 5 5 Danakil depression in central west Afar, the rift axis steps en ) echelon to the southwest into the Dabbahu segment (DVS), 4 4 L M which underwent a major dike intrusion episode during 2005– 2010 (Wright et al., 2006; Ebinger et al.,2008; Barnie et al., 3 3 2015). Nabro volcano (NVS), which erupted in June 2011, 2 2 is on the eastern margin of the Danakil depression near the Magnitude ( Eritrean–Ethiopian border (Hamlyn et al., 2014; Goitom et al., 2015; Fig. 1). 1 1 A variety of geophysical studies have shown that exten- sion in Afar and the Main Ethiopian rift is accommodated by 0 0 a combination of magmatic intrusion and lithospheric thin- 0 100 200 300 400 500 Hypocentral Distance (km) ning (e.g., Bastow and Keir, 2011).
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